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Teacher sheet · Ages 15–16 · about 45–50 minutes

Deserts: water balance, energy and adaptation

Lesson page: echoesof.science/school/deserts/ages-15-16/ · Pupil worksheet: echoesof.science/school/deserts/ages-15-16/print/

Learning aims

Lesson plan

TimeActivity
5 minStarter: rank Antarctica, the Sahara and Brussels by yearly precipitation. Discuss what makes a desert.
10 minRead the text; unit conversions (inches to mm, mm to litres, °F ranges to °C).
20 minSurface-area practical with readings every 15 minutes.
5 minAvoid or endure? game.
5 minQuiz; discuss the different definitions.

Materials for the experiment

Safety: Use only water. Keep water away from the balance's plug and socket and wipe up spills. No heaters or lamps are needed.

Common misconceptions

Pupils may think…Actually…
A temperature range in °F converts like a temperature reading (subtract 32).A difference converts by × 5/9 only: 50 °F range ≈ 28 °C range.
Deserts are caused by drought, so desertification is natural.Desertification is usually driven by deforestation and human demands on semiarid land.
Shape itself matters, not area.The rate per unit of exposed area is similar; less exposed area means slower loss.

Worksheet answers

  1. 70 × 25.4 = 1,778 mm; 160 × 25.4 = 4,064 mm. 4,064 ÷ 250 ≈ 16 times the arid limit.
  2. Loss = 24.0 − 15.6 = 8.4 g in 1.5 h, so 5.6 g/h; per 100 cm² = 5.6 ÷ 3 ≈ 1.9 g/h.
  3. By day, clear skies let at least 90% of sunlight reach the ground, so it heats strongly. At night there are few clouds and little water vapour, so about 90% of the day's heat radiates away (against about 50% in moist places), and the temperature drops sharply.
  4. Give both figures with their definitions (for example arid = less than 250 mm, with or without polar deserts) and say that the difference comes from the definition, not a measurement error.

Quiz answers

  1. In Meigs' classification, how much rain does semiarid land get a year? 250–500 mm. Semiarid land is usually steppe, not desert.[1]
  2. Cairo gets 28 mm of rain a year. How many litres fall on each square metre? 28 litres. 1 mm on 1 m² equals 1 litre.[2]
  3. A daily temperature range of 50 °F is about how big in °C? About 28 °C. A temperature difference converts as × 5/9, without the 32 offset.[4]
  4. Why do the USGS and National Geographic give different shares of land as desert? They use different definitions of a desert. Counting polar and borderline areas or not changes the total.[1][3]
  5. Why does at least 90% of sunlight reach the ground in many deserts? High pressure brings very few clouds. Clear skies let most of the Sun's rays through.[4]
  6. How do ephemeral plants survive drought? They escape it by completing their life cycle in weeks after rain. Their seeds wait in the soil until the next rain.[2]

Going further

Collect a month of daily maximum and minimum temperatures for a desert city and for your own town from a national weather service, calculate the average daily range for each and explain the difference.

Sources used in this lesson

Full list with links and a note on each source's reliability: echoesof.science/school/deserts/sources/

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